Bijoy, Nandan S; Lathika, Cicily Thomas; Padmakumar, K B; Smitha, B R; Asha Devi, C R; Sanjeevan, V N(Polish Academy of Sciences, Institute of Oceanology, 2013)
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Abstract:
The phytoplankton standing crop was assessed in detail along the South Eastern
Arabian Sea (SEAS) during the different phases of coastal upwelling in 2009.During phase 1 intense upwelling was observed along the southern transects
(8◦N and 8.5◦N). The maximum chlorophyll a concentration (22.7 mg m −3) was
observed in the coastal waters off Thiruvananthapuram (8.5◦N). Further north
there was no signature of upwelling, with extensive Trichodesmium erythraeum
blooms. Diatoms dominated in these upwelling regions with the centric diatom
Chaetoceros curvisetus being the dominant species along the 8◦N transect. Along
the 8.5◦N transect pennate diatoms like Nitzschia seriata and Pseudo-nitzschia sp.
dominated. During phase 2, upwelling of varying intensity was observed throughout
the study area with maximum chlorophyll a concentrations along the 9◦N transect
(25 mg m−3) with Chaetoceros curvisetus as the dominant phytoplankton. Along
the 8.5◦N transect pennate diatoms during phase 1 were replaced by centric diatoms
like Chaetoceros sp. The presence of solitary pennate diatoms Amphora sp. and
Navicula sp. were significant in the waters off Kochi. Upwelling was waning during
phase 3 and was confined to the coastal waters of the southern transects with
the highest chlorophyll a concentration of 11.2 mg m−3. Along with diatoms,
dinoflagellate cell densities increased in phases 2 and 3. In the northern transects
(9◦N and 10◦N) the proportion of dinoflagellates was comparatively higher and was
represented mainly by Protoperidinium spp., Ceratium spp. and Dinophysis spp.
Ramachandran Nair, P V(Cochin University of Science and Technology, May , 1974)
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Abstract:
This thesis deals with the results of investigations on primary production and related aspects conducted in the Indian seas since 1957 and includes the regional and seasonal variations in the rate of production factors controlling the same and the magnitude of potential fishery resources derived from it. Data collected for various periods using oxygen and 14c techniques from the Gulf of Mannar, palk bay, the south west coast of India including laccadive sea together with other available data form the basis of these studies.